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Data Release for Holocene Paleohydrology from alpine lake sediment, Emerald Lake, Wasatch Plateau of central Utah, USA

Dates

Publication Date
Start Date
2009
End Date
2019

Citation

Anderson, L., and Pelltier, R., 2023, Data Release for Holocene paleohydrology from alpine lake sediment, Emerald Lake, Wasatch Plateau of central Utah, USA: U.S. Geological Survey data release, https://doi.org/10.5066/P9CZFVNJ.

Summary

Holocene sediments at Emerald Lake in central Utah (3090 m a.s.l), document the paleohydroclimatic history of the western Upper Colorado River headwater region. Multi-proxy analyses of sediment composition, mineralogy, and stable isotopes of carbonate (d18O and d13C) show changes in effective moisture for the past ca. 10,000 years at millennial to decadal timescales. Emerald Lake originated as a shallow closed-basin cirque pond during the early Holocene. By ca. 7000 cal yr BP, higher lake levels and carbonate d18O values indicate rising effective moisture and higher proportions of summer precipitation continued at least until ca. 5500 cal yr BP when a landslide entered the lake margin. Between ca. 4500 and 2400 cal yr BP dry conditions [...]

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Attached Files

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emerald_lake_data_release_metadata.txt 23.61 KB text/plain
Emerald_data_dictionary.csv 6.68 KB text/csv
Emerald_CoreD_Radiocarbon.csv 2.46 KB text/csv
Emerald_Water_Chemistry.csv 288 Bytes text/csv
Utah_Lake_Water_Isotopes.csv 2.12 KB text/csv
Emerald_CoreA_density_water_carbon.csv 23.12 KB text/csv
Emerald_CoreD_density_water_carbon.csv 19.44 KB text/csv
Emerald_CoreD_xrd_mineralogy.csv 14.4 KB text/csv
Emerald_CoreD_Magnetic_Susceptibility.csv 10.73 KB text/csv
Emerald_CoreD_carbonate_isotopes.csv 18.45 KB text/csv
Emerald_Water_Column.csv 756 Bytes text/csv

Purpose

This study presents a new lake carbonate d18O paleoclimate record for the Holocene from Emerald Lake in central Utah. At 3090 m elevation, the headwater lake is on the summit of the Wasatch Plateau, which delineates the border between the Great Basin and Colorado Plateau regions. The location of Emerald Lake on the western boundary of the UCB provides a new opportunity to evaluate sub-regional snow and drought patterns within the watershed. The data show that the multi-decadal scale d18O record (~30-year average resolution) from Emerald Lake reflect changes in precipitation and evaporation by utilizing a modern lake d18O interpretive framework, and multiproxy sediment variations provide evidence for changes in lake level. Comparison with records from the eastern Great Basin and Northern Rockies approximates the geographic scale of synoptic climate patterns related to jet stream and North American Monsoon dynamics. The Wasatch Plateau has a long history of damaging landslides, including mass movement that has evidently altered the western margin of Emerald Lake. The radiocarbon-based chronology of the Emerald Lake sedimentary record provides accurate timing for a landslide event and allows evaluation of its occurrence within the context of the paleoclimatic record. csv files of: Emerald Lake core D radiocarbon ages (Table 1 in publication), Emerald Lake aqueous geochemistry and water column measurements (Table 2 in publication), Utah High Plateau surface water d18O, d2H and d-excess (Table S1 in publication), Emerald Lake core A sediment core data: density, % water, total carbon (TC) and total inorganic carbon (TIC), Emerald Lake core D sediment core data: density, % water, magnetic susceptibility, total carbon (TC) and total inorganic carbon (TIC), mineralogy by x-ray diffraction (xrd), carbonate stable isotopes (carbon and oxygen), Emerald Lake water column data.

Additional Information

Identifiers

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DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9CZFVNJ

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